Mutual replacement reactions in alkali feldspars II: trace element partitioning and geothermometry
Perthitic alkali feldspar primocrysts in layered syenites in the Klokken intrusion in South Greenland, underwent dissolution-reprecipitation reactions in a circulating post-magmatic aqueous fluid at ∼450°C, and are to a large degree pseudomorphs. These
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|Source:||Contributions to Mineralogy and Petrology (Electronic)|
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